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Coupled Optical and Molecular Insights Into Dissolved Organic Matter Dynamics in Runoff From Patchy Slopes Co‐Covered by Vegetation and Biocrusts During Rainfall in Arid and Semiarid Regions

Datos Bibliográficos

ID19236239
AutoresFei Wang (0000-0003-0860-6317, State Key Laboratory of Soil and Water Conservation and Desertification Control College of Soil and Water Conservation Science and Engineering, Northwest A&F University Yangling Shaanxi China), Guo Chen (0000-0003-2968-9633, College of Urban and Environmental Sciences, Peking University Beijing China), Jianhang Lan (State Key Laboratory of Soil and Water Conservation and Desertification Control College of Soil and Water Conservation Science and Engineering, Northwest A&F University Yangling Shaanxi China), Lihong Jia (0000-0001-5675-0650, Soil Conservation Supervision Bureau for Shanxi‐Shaanxi‐Inner Mogolia Contiguous Areas, YRCC Yulin Shaanxi China), Qingwei Zhang (0009-0003-0567-6739), Qing‐wei Zhang (0000-0003-2589-2896, State Key Laboratory of Soil and Water Conservation and Desertification Control College of Soil and Water Conservation Science and Engineering, Northwest A&F University Yangling Shaanxi China), Fengbao Zhang (0000-0003-1003-256X, State Key Laboratory of Soil and Water Conservation and Desertification Control College of Soil and Water Conservation Science and Engineering, Northwest A&F University Yangling Shaanxi China), Jian Wang (0000-0001-6128-1254, State Key Laboratory of Soil and Water Conservation and Desertification Control College of Soil and Water Conservation Science and Engineering, Northwest A&F University Yangling Shaanxi China), Yi-Xiang Wang (0000-0001-5697-0717, Institute of Soil and Water Conservation), Yu Pang (0000-0002-0379-1085, Department of Ocean Science and Center for Ocean Research in Hong Kong and Macau The Hong Kong University of Science and Technology Hong Kong China), Ming Li (0000-0001-7109-5084, College of Natural Resources and Environment, Northwest A&F University Yangling Shaanxi China), Ding He (0000-0002-5097-9953, Department of Ocean Science and Center for Ocean Research in Hong Kong and Macau The Hong Kong University of Science and Technology Hong Kong China), Hao Wang (0000-0003-3392-1562, State Key Laboratory of Soil and Water Conservation and Desertification Control College of Soil and Water Conservation Science and Engineering, Northwest A&F University Yangling Shaanxi China, autor de correspondencia)
Año2026
Fecha de publicación2026-04-27
Peer ReviewedSí
Open AccessSí
TipoARTICLE
RevistaLand Degradation and Development (JOURNAL)
Identificadores de la revistaISSN: 1085-3278 • E-ISSN: 1099-145X
EditorialWiley (PUBLISHER • GB)
DOI10.1002/ldr.70630
OpenAlexW7156826438
IdiomaEN
Referencias citadas68

Arid landscapes are shifting from biocrusts‐ or vascular plant‐dominated systems to mosaics where both coexist under climate change; yet, dissolved organic matter (DOM) dynamics in these transitional habitats remain poorly understood. Therefore, three types of runoff plots were set on slopes with biocrusts (BC), Bothriochloa ischaemum (L.) + biocrusts (BI BC ), and Artemisia sacrorum Ledeb. + biocrusts (AS BC ) in a typical semiarid region. The dynamics of DOM in surface runoff were analyzed by simulated rainfall experiments coupled with optical techniques and Fourier transform ion cyclotron resonance mass spectrometry (FT‐ICR MS). Overall, the DOM loss rates in the BI BC and AS BC were significantly reduced compared to the BC. Runoff from all runoff plots was dominated by the DOM with protein‐like components (34% to 96%). Runoff from the BC was characterized by a 1.48‐ to 2.08‐fold higher proportion of humic‐like components compared to BI BC and AS BC , accompanied by greater aromaticity and a higher degree of humification. DOM in runoff across all runoff plots was dominated by CHO compounds (52%), with highly unsaturated compounds as the primary constituents (52%). DOM in the runoff from the BC exhibited more stable molecular structures and stronger aromaticity, whereas those from the AS BC showed a higher proportion of multi‐heteroatomic components such as CHONP and CHONS. In conclusion, herbaceous vegetation and biocrusts form composite patches that regulate DOM transport and loss by modifying its quantity, composition, and stability. These processes have important implications for water quality and carbon cycling in arid landscapes. This study also highlights the synergistic value of integrating optical and molecular techniques to advance understanding of ecosystem‐scale DOM dynamics

Arid · Dissolved organic carbon · Erosion · Organic matter · Surface runoff · Aquatic Ecosystems and Phytoplankton Dynamics · Biocrusts and Microbial Ecology · Plant Water Relations and Carbon Dynamics

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